AOML
NOAA

Meridional Overturning Circulation

South Atlantic Meridional Overturning Circulation

South Atlantic Meridional Overturning Circulation: Pathways and Modes of Variability

PIs: Renellys Perez and Silvia Garzoli

Collaborators: Ricardo Matano, Rym Msadek

Previous observational and modeling efforts on the meridional overturning circulation (MOC) have been focused on the North Atlantic and the Southern Oceans, which are the preferential sites for deep-water formation. To understand the feedbacks between the North Atlantic and the Southern Oceans we need to improve our understanding of the pathways of the upper and lower limbs of the MOC in the South Atlantic (SA) Ocean, which are the most important links between them. The SA is not just a passive conduit for the transit of remotely formed water masses, but actively influences them through air–sea interactions, mixing, subduction, and advection. Therefore, we are characterizing the pathways of the upper and lower limb of the MOC in the SA and identify the dynamical mechanisms that control these pathways. The study focuses on identifying the natural modes of variability in the SA and their impact on the MOC. Our research focuses on the analysis of state-of-the-art eddy-permitting and eddy-resolving NOAA/GFDL climate model simulations. Specifically, we use a suite of experiments done with the CM2.5 and CM2.6 coupled models, which were forced with present day conditions and different climate change scenarios. These simulations will be compared against the non-eddying Coordinated Model Intercomparison Project and Intergovernmental Panel on Climate Change Fifth Assessment Report models including the NOAA/GFDL coarse resolution models (CM2.1, CM3), a suite of process-oriented numerical experiments using regional ocean models, and global in-situ and satellite observations.

Figure - The low-frequency modes of variability in the SA: a) schematic of the proposed modes; b) first EOF of the SSH AVISO data and its associated geostrophic circulation (courtesy of R. Matano).